Study Questions Exam 2
1. The height of capillary rise in a tube of radius X is Y. What is the rise in a tube of
radius 0.1X?
Height of rise is inversely proportional to tube radius. H / Y = X / 0.1X, so H = 10Y.
2. What are the components of soil water potential under saturated conditions? Under
unsaturated conditions?
Saturated, gravitational + pressure + osmotic; unsaturated, gravitational + matric +
osmotic.
3. In the absence of a semipermeable membrane, does osmotic potential affect water
flow in soil?
No. That’s why only gravitational + pressure (or matric) potentials affect flow in
saturated (or unsaturated) soil. Osmotic potential will, however, affect flow to roots.
4.
What two soil water variables are related in a soil moisture characteristic curve?
Water content and matric potential (also called tension or suction).
5. Given a soil moisture characteristic curve for a clay and a sand, distinguish
between the two soils. Which has the higher water content at saturation? Which shows
the steeper decrease in water content with decreasing (more and more negative) matric
potential? How is this behavior related to pore size distribution?
Since the bulk density of a clay is typically less than the bulk density of a sand, there is
typically greater pore space in a clay. Consequently, a clay has higher water content at
saturation (0 matric potential). Furthermore, a clay has a wider distribution of pore sizes
than a sand, which mostly has large pores. Thus, when a sand drains from saturation
under increasing tension (more and more negative matric potential), its water content
decreases quickly whereas the decrease in water content of a clay under increasing
tension is less steep.
6.
What effect does structure have on the soil moisture characteristic curve?
Distinguish between a curve for a structured and compacted soil.
Structure may increase total pore space and does increase the amount of
macroporosity (fraction of pore space composed of large pores). Thus, a structured soil
gives a moisture characteristic curve that has higher water content at saturation and
steeper decrease in water content with increasing tension than a compacted soil (which
has less macroporosity).
7. The soil moisture characteristic curve shows different branches depending on
whether the soil is absorbing water or draining. What is the phenomenon called?
Distinguish which branch is for absorption and which for drainage. Give a reason for
this behavior.
Hysteresis. For the same matric potential, the moisture characteristic curve for a soil
that is draining from saturation shows higher water content than the same soil when it is
wetting. The phenomenon is thought to be due to several factors, including “ink bottle”
shape of pores. When a water-filled, bulbous pore is subject to drainage, it will not
empty until the matric potential becomes sufficiently negative that a pore of the neck
radius empties. On the other hand, the same pore will not fill when wetting until a less
negative matric potential, equal to that associated with the larger radius interior of the
pore, is reached.
8. A 50 cm3 core sample of moist soil weighed 68 g. After drying at 105 C for 24 h it
weighed 60 g. What was the gravimetric water content of moist soil? The volumetric
water content?
GW = 8 g / 60 g = 0.13
VW = [8 g / (1.0 g cm-3)] / 50 cm3 = 0.16
9. Water flow, whether saturated, unsaturated or vapor phase, is always from higher
to lower potential (True / False)?
10.
Work a simple saturated flow problem, like from lab.
See examples for lab exam.
11. What effect does texture have on the saturated hydraulic conductivity? What
effect does structure have? Explain in terms of pore sizes.
Saturated hydraulic conductivity increases with increasing coarseness of texture.
Conductivity of a structured soil is typically greater than in a soil without structural units.
In both cases, the effect is due to increasing fraction of large pores, either in increasing
coarseness or presence of large interaggregate pores.
12.
Is matric potential more important than gravitational potential in causing
unsaturated water flow?
Yes. This can easily been seen using the approximate relationship, 1 bar = 1000 cm
water. For example, if the surface soil is fully saturated (matric potential = 0 bar) and
soil 10 cm below is at field capacity (matric potential = -0.3 bar), the difference in total
potential, surface minus subsurface, is [0 cm (gravitational potential) + 0 cm (matric
potential)] – [ -10 cm (gravitational potential) + (-300) cm (matric potential)] = 310 cm.
Thus, the gradient in water potential, difference in potential divided by distance, 31, is
predominantly due to the difference in matric potential.
13. Why does the unsaturated hydraulic conductivity decrease with decreasing water
content?
There are 3 main reasons: 1) the water-filled cross section decreases with decreasing
water content ; 2) the path through which water flows increases with decreasing water
content; and 3), most importantly, the size of the pores that remain filled with water
decreases with decreasing water content. Recall that resistance to flow increases with
decreasing pore radius (small pore area compared to perimeter).
14.
The direction of vapor phase water movement in soil is from
Lower to higher vapor pressure
Cold soil to warm soil
Saline to nonsaline soil
Low to higher matric potential
True or False
True or False
True or False
True or False
Water vapor moves down a vapor pressure gradient so that since vapor pressure is
greater under warm temperature and above nonsaline water, the first through third
statements are false. Furthermore, when the soil is very dry, soil solids hold liquid water
with such tenacity that its vapor pressure is reduced.
15. What effect does a layer of clay under coarser texture soil have on water
movement? Conversely, what effect does a layer of sand under finer texture soil have
on water movement?
An underlying clay layer with its comparatively low hydraulic conductivity will slow water
movement. Interestingly, something of the same thing occurs when water moving
through a fine texture soil encounters a layer of coarse material. Obviously, the coarse
layer cannot accelerate water flow since this is controlled by the hydraulic conductivity
of the overlying fine texture soil. However, the coarse layer does have an effect. The
water in the fine pores of the overlying fine texture soil is held at too great of tension
(too negative matric potential) to enter the large pores of the underlying coarse soil.
Therefore, water tends to build up above the coarse soil and will not enter it until the
tension on the water in the fine soil becomes much lower. It is in this way that the sand
layer temporarily retards water flow.
16. What is field capacity? Since water is soil is always moving, what is really meant
by this term?
Field capacity is water content at approximately -0.3 bar tension (also this value of
water tension). The concept stems from the observation that water drainage becomes
quite slow at about -0.3 bar tension and, from a practical standpoint, most of the water
held in the soil at this tension will not drain deeper into the soil and, therefore, be
available to plants.
17.
Define wilting point, hygroscopic coefficient, and plant-available water.
Wilting point is approximately -15 bar. This is the approximate tension (matric potential)
below which plants cannot extract water sufficient to meet transpirational demand.
Hygroscopic coefficient is approximately -30 bar, the tension of water in air-dry soil.
Plant-available water is water in between field capacity and wilting point.
18.
What is gravitational water and why isn't it also considered plant-available?
Gravitation water is water in the soil at tensions above field capacity. Most of it will
drain below the root zone and so will not be available for plant uptake.
19.
What are capillary water and hygroscopic water?
Capillary water is water held in capillaries (soil pores). Like these other older,
qualitative terms, it is not a precise concept. Think of it as any soil water present when
the soil is not air-dry. In an air-dry soil, water is present only as thin, adsorbed films on
solid particles. In a somewhat wetter soil, the tiniest of pores (tiniest of capillaries) will
be water-filled.
20. Explain the effect of soil texture on plant-available water.
organic matter have on plant-available water?
What effect does
See figures in lecture synopsis. Water content at field capacity increases with
increasing fineness of texture. Similarly, water content at the wilting point increases
with increasing fineness of texture. However, these two curves at first diverge
(beginning with sand texture, going to loamy sand) but later tend to converge (heading
to clay texture). Therefore, at an intermediate texture (silt loam) the difference between
field capacity and wilting point is greatest, or, in other words, plant-available water is
greatest.
For a set texture, however, both water content at field capacity and wilting point
continue to diverge with increasing organic matter content –plant available water
increases with increasing organic matter content.
21. Draw a diagram that shows the water movement processes that comprise the field
water cycle.
See figure in lecture synopsis.
22. Explain why all rainfall at an intensity greater than the saturated hydraulic
conductivity of a soil may, for some period of time, infiltrate the soil but with continued
rainfall, infiltration slows and surface ponding develops.
Imagine the surface (~ 1 cm) soil is saturated but the soil 10 cm below the surface is
dry. In this situation there is a huge water potential gradient (see discussion # 12).
With further infiltration, however, the water content 10 cm below the surface increases
and the tension on it decreases so that the water potential gradient is reduced.
According to Darcy’s Law, it is possible to have water flow greater than the saturated
hydraulic conductivity provided that the water potential gradient is large. Thus, it is
possible to have infiltration match rainfall intensity for a period of time even though
rainfall intensity exceeds saturated hydraulic conductivity. However, the water potential
gradient will decrease to the point that rainfall intensity exceeds infiltration, resulting in
ponding and runoff.
23. What effect does the soil surface hydraulic conductivity have on infiltration? How
does formation of a surface crust affect infiltration?
A thin layer of low hydraulic conductivity soil at the surface (a crust) will limit the rate of
infiltration, not a good thing.
24.
What effect does soil water content at the onset of infiltration have on infiltration?
See discussion # 12 and # 22. Higher water content at onset of infiltration means
smaller gradient in water potential at the soil surface. Thus, if rainfall intensity is greater
than saturated hydraulic conductivity, the period of time during which infiltration rate can
match rainfall intensity is shorter and there is more runoff.
25. What meteorological factors influence combined evaporation and transpiration
(evapotranspiration)?
Solar radiation, water vapor pressure (humidity), wind speed and temperature.
26. Evaporation from soil may proceed at a constant rate that is determined by
environmental conditions and meet demands set by external evaporativity. But after the
soil sufficiently dries, the rate of evaporation tapers off. Explain why.
The answer is similar to # 22. Consider a uniformly wet soil. As water evaporates from
the surface, a large gradient in water potential –higher just below the surface and much
lower at the surface—is established. This gradient is sufficient to bring water from
deeper in the soil to the surface where it evaporates. But as evaporation continues, the
soil dries to a deeper depth and the gradient in water potential decreases (the distance
over which a large difference in water potential exists becomes longer). Eventually, the
decreasing water potential gradient is insufficient to move water to the surface fast
enough to meet demands set by external evaporativity and the rate of evaporation
decreases.
27. How do mulches (including crop residue left on the surface by conservation tillage)
reduce evaporative losses of soil water?
They reduce solar radiation, gradient in water vapor pressure (extending from the soil
surface upward into the air), wind speed at the soil surface and temperature –all factors
that favor evaporation.
28. What effect does shading the soil surface by a plant canopy have on the relative
contribution of transpiration and evaporation to overall evapotranspiration?
Decreases evaporation, therefore, increases contribution of transpiration.
29.
Is percolation more common when infiltration exceeds evapotranspiration?
Yes. Water that infiltrates the soil may either move downward or be lost by evaporation
and transpiration. Thus, if evapotranspiration is less than infiltration, the tendency is for
water to percolate downward.
30.
What is the potential effect of macropore flow on ground water quality?
Macropore flow (or by-pass flow) is an avenue for rapid movement of water in the soil.
Furthermore, flow through macropores has much less contact with soil solids than flow
through micropores. Consequently, potential ground water contaminants move quickly,
with little adsorption to retard them, during macropore flow. Fortunately, macropore flow
is usually a small fraction of total water flow in soil (other than very sandy soils).
31.
What is a capillary fringe and why does it exist?
Capillary fringe refers to a water-saturated zone in the soil in which the water is at less
than atmospheric pressure (under tension or negative matric potential). It exists
because soil pores are sufficiently small that they remain filled with water under small
tension.
32.
Is the vadose zone saturated or unsaturated?
It is unsaturated by definition.
33.
What is the purpose of surface drainage? Subsurface drainage?
The purpose of both is to improve aeration in the root zone but it has the additional
benefits of allowing the soil to warm faster in the spring and allowing sooner access by
equipment after heavy rainfall.
34.
What is the importance of drainage with irrigation?
Though not discussed in class, it is important to have good drainage when using
irrigation so as to avoid accumulation of salts in the root zone. If irrigation water did not
drain but moved upward due to surface evaporation, the load of salt in each irrigation
event would stay in the root zone, ultimately creating a saline soil (discussed later in
course). When drainage is good, more water than is needed by the crop can be applied
so salt residue from the previous irrigation is leached below the root zone as water
percolates downward.
35. Name the three general types of irrigation systems. List principal advantages and
limitations of each.
Surface
Sprinkler
Drip
36.
Low cost but non-uniform wetting and inefficient water use
Higher cost but uniform wetting and efficient water use
High cost and maintenance but most efficient water use
Compare the composition of soil air to that of the atmosphere.
Compared to the above ground atmosphere, soil air is typically lower in oxygen, higher
in carbon dioxide and higher in water vapor.
37. Why is gas diffusion much smaller in soil than in air? What effect does high soil
moisture have on gas diffusion in soil?
It must pass through soil pores, along whatever circuitous path they take, often
interrupted by water-filled pores. Since the rate of gas (molecules) diffusion through
water is much slower than through air, gas diffusion in a wet soil is much slower than in
a dry soil.
38.
What happens to the redox potential when the oxygen content of soil decreases?
It decreases.
39. Under anaerobic conditions, the activity of aerobic microbes drops off and the
activity and populations of anaerobic microbes greatly increases. What do anaerobic
microbes use as terminal electron acceptors in respiration? Give a couple of examples.
Arrange in approximate order of decreasing redox potential.
Different anaerobic organisms use nitrate (NO3-), oxidized iron (Fe3+), oxidized
manganese (Mn4+), sulfate (SO42-) and carbon dioxide (CO2) as terminal electron
acceptors in respiration. When oxygen is depleted the Eh (redox potential) is favorable
for those organisms that use nitrate to flourish, and as they do the Eh is further reduced
and nitrate depleted. Then come into play those anaerobic organisms that use the
other terminal electron acceptors in the sequence given above.
40. What effect does soil organic matter have on the tendency of water-logged soils to
become strongly anaerobic?
All heterotrophic microorganisms, including anaerobes, need organic matter for energy
and as a carbon source. With little organic matter there would be little metabolic
activity, consuming oxygen or any of the other terminal electron acceptors (# 39).
Consequently, water-logged conditions would not result in strongly anaerobic conditions
without the presence of organic matter.
41.
List two ill-effects of anaerobic conditions on plant growth.
Less energy for growth, toxic products, reduced nutrient availability and others.
42.
List a few benefits of wetland soils.
For those of us in South Louisiana, protection from coastal flooding is a plus. But even
in upland areas, wetlands often control and limit downstream flooding. Other important
functions include benefit on water quality (for example, reduction in nitrate concentration
due to anaerobic respiration) and wildlife habitat / diversity. The latter is important to
our use of wetlands for recreation and fisheries.
43. On what three general criteria are wetland soils delineated and boundaries drawn
with respect to adjacent non-wetland soils?
Surface hydrology, plants and indicators of hydric soils.
44.
Roughly define hydric soils.
Soils wet sufficiently long when the temperature is high that anaerobic conditions exist.
45.
What are the usual colors expected for a well-drained soil? A poorly-drained soil?
Red, orange and brown for well-drained soil but yellow and especially gray, even bluish,
for poorly-drained soil. The gray to blue color, due to chemically reduced iron (Fe2+)
characterizes gley. Poorly-drained soils also typically contain more organic matter than
well-drained soils. Thus, poorly-drained soils may be darker.
46. List and briefly discuss three redoximorphic (colors associated with presence,
absences or distribution of oxidized and reduced iron) features of hydric soils.
Gley
Iron in chemically reduced form (see # 45)
Iron concentration Reduced iron is re-oxidized to Fe3+ and segregates to form reddish
or brownish mottling against a gray or lighter colored matrix
Iron depletion
Iron that is solubilized to Fe2+ is swept from the soil by water
moving through the soil, leaving the soil light in color.
47. Although dark colored soils absorb more solar radiation than light colored soils,
warming may be slower. Why?
See # 45. Although darker in color, the soil may be wet. Higher water content gives a
higher specific heat and increased evaporation, both tending to keep a soil cooler.
48.
How do slope and aspect affect soil temperature?
The orientation of the (bare) soil surface with respect to incident solar radiation controls
the intensity of radiation at the surface (perpendicular to radiation, greatest).
49.
In what three ways does soil water affect soil temperature?
Increased water content increases the specific heat of the soil, increasing the amount of
heat needed to raise the soil temperature a given amount. It also increases the rate of
evaporation, with increases the rate at which heat is removed from the soil by
evaporation (heat of evaporation). Increased water content also increases the thermal
conductivity so that heat absorbed at the surface is more readily transmitted deeper.
50.
Which conducts heat more readily, a dry soil or a wet soil?
See # 49.
51. Two soils are identical in all respects except that soil A has a volumetric water
content of 0.2 whereas soil B has a water content of 0.4. Which soil warms faster?
The one with the lower water content, soil A (see # 49).
52. Compare the daily temperature variation at a depth of 2 cm to the daily
temperature variation at a depth of 30 cm in soil.
The diurnal variation in temperature is greater at the surface, higher high, lower low.
Also, the timing of temperature maxima and minima are different at 2 cm and at 30 cm
depth. The extremes occur later at 30 cm than at 2 cm. This is a matter of heat
conduction into and out of the soil.
53. Compare the season temperature variation at a depth of 2 cm to that at a depth of
30 cm in soil.
This is similar to daily variation, with greater range in temperature at 2 cm than 30 cm
and annual cycles offset somewhat.
54. What is the effect of a surface mulch (including crop residues in conservation
tillage) on soil temperature?
It insulates the soil, moderating temperature compared to bare soil.